The thin-skin Sevier and thick-skin Laramide belts of the North American Cordillera provide
a long-term record of the interrelations between evolving styles of mountain building and …

Continents, especially their Archean cores, are underlain by thick thermal boundary layers
that have been largely isolated from the convecting mantle over billion-year timescales, far …

Arc volcanism across Iran is dominated by a Paleogene pulse, despite protracted and
presumably continuous subduction along the northern margin of the Neotethyan ocean for …

Mechanical properties of lithosphere are of primary importance for interpretation of
deformation at all spatial and time scales, from local scale to large-scale geodynamics and …

The Eocene epoch in the Great Basin of western North America was a period of profuse
magmatism and hydrothermal activity. During that period, the Carlin-type gold deposits in …

During the subhorizontal (flat) subduction of an ocean–lithosphere plate, the overlying
continental plate is deformed far inland of the plate boundary. In addition, arc magmatism …

Two fundamentally different orogenic systems have existed on Earth throughout the
Phanerozoic. Circum-Pacific accretionary orogens are the external orogenic system formed …

There has been much debate recently concerning the long-term (ie,> 1 my) strength of
continental lithosphere. In one model, dubbed jelly sandwich, the strength resides in the …

Mantle seismic structure beneath the United States spanning from the active western plate
margin to the passive eastern margin was imaged with teleseismic P and S wave traveltime …

Continental arcs in Cordilleran orogenic systems display episodic changes in magma
production rate, alternating between flare ups (70–90 km 3 km− 1 Myr− 1) and lulls (< 20 km …